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Tytuł:
Związek akumulacji śniegu na lodowcach północno-zachodniego Spitsbergenu z cyrkulacją atmosferyczną, opadami i temperaturą powietrza w okresach zimowych
Relation between the snow accumulation on glaciers of North-West Spitsbergen and the atmospheric circulation, precipitation and air temperature in the winter seasons
Autorzy:
Grabiec, M.
Powiązania:
https://bibliotekanauki.pl/articles/260836.pdf
Data publikacji:
2003
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Spitsbergen
akumulacja śniegu
cyrkulacja atmosferyczna
opady
temperatury powietrza
snow accumulation
atmospheric circulation
precipitation
air temperature
Opis:
This work attempts to determine connections between glaciers' winter mass balance and meteorological factors of winter seasons. Detailed analysis was carried out between the snow accumulation of Austre Broggerbreen and the meteorological data from Ny-Alesund station (Kongsfjord region) from 1975 to 1998. Relation has been found between the snow accumulation and warm and humid air masses frequency in winter seasons (X - V). Those masses are mainly from southerly and southwesterly directions for Svalbard. The winter mass balance shows very clear connection with air temperature and precipitation factors of winter seasons (sum of winter precipitation, number of days with precipitation intensity >= 5 mm per day, winter mean air temperature, and number of days with maximum daily air temperature >= 0°C). A particularly close connection is observed between winter mass balance and number of days with precipitation intensity >= 5 mm per day at the positive daily maximum air temperature (LPTmax) (r = 0.81) - Fig. 8. The winter mass balance multiply regression (Wb) was worked with the use of the elementary meteorological factors: the average winter temperature (T) and the sum of precipitation in the same period (P). On the basis of the multiply regression of winter balance it is possible to predict snow accumulation changes. Over the next 50 years the winter snow accumulation of Austre Broggerbreen could increase about 15% if the scenario of climatic changes by Hanssen-Bauer (2002b) is used. If, in addition, one assumes the stability of ablation, the mass balance of glaciers will rise by 24%, but the mass balance will still be negative.
Źródło:
Problemy Klimatologii Polarnej; 2003, 13; 161-171
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie wilgotności względnej i opadów atmosferycznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010
Differentiation of relative humidity and precipitation in the Forlandsundet region (NW Spitsbergen) in the summer 2010
Autorzy:
Araźny, A.
Przybylak, R.
Kejna, M.
Powiązania:
https://bibliotekanauki.pl/articles/261033.pdf
Data publikacji:
2011
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
topoklimat
wilgotność względna
opady atmosferyczne
cyrkulacja atmosferyczna
Spitsbergen
Forlandsundet
topoclimate
relative humidity
precipitation
atmospheric circulation
Opis:
W artykule przedstawiono zróżnicowanie wilgotności względnej powietrza oraz opadów atmosferycznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim (21 VII - 31 VIII) 2010 roku. Do analizy wzięto cogodzinne dane wilgotności względnej (z 18 stanowisk) oraz sumy opadów atmosferycznych z okresów 1-3 dniowych (z 11 stanowisk). Dla obydwu badanych elementów meteorologicznych stwierdzono znaczne przestrzenne zróżnicowanie ich wartości uwarunkowane rodzajem podłoża, wysokością nad poziom morza, odległością od morza, ekspozycją oraz lokalną cyrkulacją atmosferyczną. Zbadano wpływ cyrkulacji atmosferycznej na wartości wilgotności względnej i opadów atmosferycznych korzystając z kalendarza typów cyrkulacji dla Spitsbergenu.
In the paper some main results concerning spatial differentiation of relative humidity and precipitation in the Forlandsundet region (NW Spitsbergen) in summer season (21 VII - 31 VIII) of 2010 are presented (Table 1, Figs 1-2). For analysis hourly data from 18 and 11 sites, respectively for relative humidity and precipitation have been used. Relative humidity was measured using automatic weather stations Davis Ventage Pro2 and MadgeTech sensors. On the other hand, for measurements of precipitation Hellmanns' ombrometers and automatic weather stations Davis Ventage Pro2 have been utilised. Large spatial differences of relative humidity and precipitation noted in the study area were influenced by different factors, e.g. character of ground, altitude above sea level, distance from the sea coast, exposition to the sun and incoming air masses, and local atmospheric circulation. Highest mean values of relative humidity (94.6%) occurred at the site surrounded by the sea (Sarstangen Peninsula, SAT), while the lowest one (86.4%) at the site located 200 m from the Waldemar Glacier termini (ATA) (Table 3, Fig. 3). The first half of the day saw highest values of relative humidity than the second one (Fig. 4). The reason of this may be explained by the opposite daily course of air temperature. Daily courses are getting more and more clear in line with decreasing value of cloudi-ness (Fig. 5). In the Forlandsunet region most frequent were air masses which can be described as humid and very humid. Days with moderate dry and dry air were noted very rarely (Fig. 6). Relative humidity shows usually very high and statistically significant correlation between data from the analysed sites (Table 3). Weak and not statistically significant correlations (r < 0.3) were calculated only between the following pair of sites SAT-PH2 and SJ1-PH2. In the summer 2010 the lowest total of precipitation (8.5 mm) in the KH station, out of all Toruń Polar Expeditions since 1975, have been observed (Table 4). In the firn part of the Waldemar Glacier seasonal total of precipitation was 3-4 times greater than in sites located on coastal plains. In the Kaffioyra Plain and Waldemar Glacier region vertical lapse rate was twofold greater between KH and LW1 than between KH and LW2 (14.7 and 7.7 mm/100m, respectively). In the entire study area, highest summer total of precipitation occurred in the middle part of the Prins Karls Forland island. Relationships between atmospheric circulation and relative humidity as well as precipitation were investigated using data from the KH station and calendar of daily synoptic types for Spitsbergen constructed by Tadeusz Niedźwiedź (Table 5). The most humid conditions in the summer 2010 were observed during inflow of air masses from south-western direction (6.6% above summer mean), while most dry air (-9.7%) - from the north-eastern direction. Similar relationships have been found for precipitation. Analysis of relationships occurring between direction of winds and relative humidity data confirms also the above results. Highest values of relative humidity (>90%) were observed during winds inflowing from the southern sector, while the lowest ones - from the north-eastern direction (Fig. 7).
Źródło:
Problemy Klimatologii Polarnej; 2011, 21; 155-172
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie termiki gruntu na Równinie Kaffiöyra (NW Spitsbergen) w lecie 1997 i 1998 w porównaniu z okresem 1975-98
Differentiation of soil temperature on the Kaffiöyra Plain (NW Spitsbergen) in summer 1997 and 1998 in comparison to the period 1975-98
Autorzy:
Araźny, A.
Powiązania:
https://bibliotekanauki.pl/articles/260959.pdf
Data publikacji:
2001
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
termika gruntu
temperatura gruntu
Spitsbergen
soil temperature
Opis:
The paper presents the results of soil temperature measurements on the Kaffiöyra Plain from the polar summer period 1997 (Tab. 1) and 1998 (Tab. 2) compared to the period 1975-1998 (Tab. 3). The soil temperature measurements were carried out on three ecotops: on the sandy beach, on end moraine of the Aavatsmark Glacier, and on tundra (Fig. 1). The measurements were taken daily at 01, 07, 13 and 19 LMT at depths: 1, 5, 10, 20 and 50 cm by soil thermometers. The thermal characteristics of soils at different ecotops differ by physical characteristics, moisture, degree of vegetation cover and thickness of active layer. The paper presents the question of thermal changes in the soil with general weather conditions. The 1997 summer was very wet, strong winds domination and mean sunshine. The 1998 summer, on the contrary, was more cloudy and warmer, and the atmosphere dynamics lower with rare light rainfall (Fig. 2, Tab. 4). The comparison of summer seasons was made for the common period 21 July - 31 August. The thermal changes of the soil on the Kaffioyra Plain are best illustrated by the data from the beach because observations at this stand were made during all of the expeditions. The mean temperature at all depth was the lowest in 1982 and 1997, the highest in 1985 and 1998 (Fig. 5). In the analysed period the measurement point on the beach was the coldest stand, tundra was warmer, and the stand on the moraine the warmest (Tab. 3, Fig. 4).
Źródło:
Problemy Klimatologii Polarnej; 2001, 11; 81-92
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie temperatury i wilgotności wyględnej powietrza w rejonie Kaffiøyry (NW spitsbergen) w sezonie letnim 2014 roku
Spatial differentiation of air temperature and relative air humidity in the Kaffiøyra region (NW Spitsbergen) in summer season 2014
Autorzy:
Kejna, M.
Ulandowska-Monarcha, P.
Strzyżewski, T.
Powiązania:
https://bibliotekanauki.pl/articles/260765.pdf
Data publikacji:
2015
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
pionowe gradienty temperatury powietrza
pionowe gradienty wilgotności powietrza
stany równowagi termodynamicznej atmosfery
topoklimat
Kaffiøyra
Spitsbergen
lapse rate of air temperature and relative humidity
thermodynamic equilibrium state
topoclimate
Kaffioyra
Opis:
W artykule przedstawiono zróżnicowanie przestrzenne temperatury oraz wilgotności powietrza w rejonie Kaffiøyry (NW Spitsbergen) w sezonie letnim 2014 r. Na podstawie pomiarów na stanowiskach położonych na różnych wysokościach nad poziomem morza przeanalizowano zmiany temperatury i wilgotności powietrza w pionie, obliczono pionowe gradienty tych elementów. Uzyskane wyniki odniesiono do pionowych sondaży atmosfery wykonywanych w pobliskiej stacji w Ny Ålesund. Temperatura oraz wilgotność względna powietrza wykazują znaczne zróżnicowanie przestrzenne. Relacje między stanowiskami zmieniają się z dnia na dzień w zależności od rodzaju mas powietrza oraz zachmurzenia. Stwierdzono również zmienność pionowych gradientów temperatury i wilgotności względnej powietrza w cyklu dobowym.
This article presents the spatial diversity of temperature and relative humidity of the air in the area of Kaffiøyra (NW Spitsbergen). In the summer season of 2014 (21 July – 31 August), observations were carried out at 9 measurement points equipped with temperature and humidity recorders. The points were located in two terrain profiles: the mountains where the highest point was situated at 590 m a.s.l. in the Prins Heinrichfjella range and from the terminal moraines to the firn field (375 m a.s.l.) of the Waldemar Glacier. On the basis of the measurements taken at the sites situated at different absolute heights vertical changes in air temperature and humidity were analysed and lapse rate of air temperature gradients were determined. The results were referenced to vertical atmospheric soundings carried out at the nearby station in Ny Ålesund. The air over NW Spitsbergen (Ny Ålesund) demonstrated a mean vertical lapse rate of 0.61˚C/100 m at the atmospheric layer up to six or seven hundred metres. On most days normal stratification was observed, where temperature fell with height, on 3 days a ground-level air temperature inversion occurred and on 9 days a temperature inversion occurred in the free troposphere. In the area of Kaffiøyra, air temperature decreased with height from 5.5°C on the coast (KH) to 2.5°C at 590 m a.s.l. (PH2). On the Waldemar Glacier, the mean air temperature ranged from 5.0°C on the moraines (ATA) to 3.6°C on the firn field (LW2). The relationship between the sites changed on a daily basis, depending on the cloud amount, insolation and local circulation (e.g. connected with the influence of foenic wind). Averaged lapse rate in relation to the coast (KH) reached between 0.84°C/100 m (LW1-KH) and 0.39°C/100 m (KU-KH) or 0.40°C/100 m (ATA-KH). The mountain tops (PH1 and PH2) are also distinguished by their smaller lapse rate. An inversion in the vertical distribution of air temperature was also frequent and, for example, at the KT site it occurred at 33.9% of the hours and at 28.7% at ATA. On the Waldemar Glacier, inversion occurred at a frequency of 16.3% at its front (LW1) to 8.8% at its firn field (LW2). On the mountain tops, the inversion occurred at a frequency of 18% (PH2). The relative humidity of the air over Spitsbergen is high due to the prevalence of maritime air masses. According to the soundings conducted at Ny Ålesund, the humidity increased with the height, however in 13 cases a vertical inversion of relative humidity occurred – the overground air layers proved more saturated with water vapour. On Kaffiøyra, the average relative humidity of the air was 87.7% and increased up to approx. 500 m, above which it slightly dropped. This results from a high frequency of occurrence of Stratus clouds which do not reach the higher tops. The vertical gradients of relative humidity were diverse: at most sites, the relative humidity increased with the height, for example at the PH1 site, the gradient was 3.12%/100 m. A greater diversity of the relative humidity was typical of the hours around midday.
Źródło:
Problemy Klimatologii Polarnej; 2015, 25; 211-226
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie przestrzenne wilgotności względnej powietrza w północnej części równiny Kaffiøyra i na Lodowcu Waldemara (NW Spitsbergen) w okresie od września 2010 do sierpnia 2013
Spatial diversity of air relative humidity in the northern part of the Kaffiøyra plain and the Waldemar Glacier (NW Spitsbergen) from September 2010 to August 2013
Autorzy:
Przybylak, R.
Araźny, A.
Ulandowska-Monarcha, P.
Powiązania:
https://bibliotekanauki.pl/articles/260842.pdf
Data publikacji:
2014
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Arktyka
Spitsbergen
klimat
wilgotność względna powietrza
cyrkulacja atmosferyczna
Arctic
climate
relative air humidity
atmospheric circulation
Opis:
W artykule przedstawiono zróżnicowanie przestrzenne wilgotności względnej powietrza w północnej części rejonu Kaffiøyry i na Lodowcu Waldemara w okresie IX 2010 – VIII 2013. W okresie od września 2010 do sierpnia 2011, dla którego istnieją najpełniejsze dane dla wszystkich stanowisk pomiarowych, najwyższe wartości wilgotności względnej zostały zanotowane na szczytach górskich (89%) i na polu firnowym Lodowca Waldemara (86%). Najniższa wartość tego parametru wystąpiła natomiast na tundrze (79%). W całym okresie badawczym, na podstawie zredukowanej liczby stacji, stwierdzono, iż najsuchszy był punkt Kaffiøyra-Heggodden (KH, 83%) zlokalizowany na morenie czołowo-bocznej Lodowca Aavatsmarka, a najbardziej wilgotno było na polu firnowym Lodowca Waldemara (LW2, 85%). Wilgotność względna na badanym obszarze wykazała przeważnie wzrost wartości wraz ze wzrostem wysokości nad poziom morza. Najwilgotniejsze powietrze w rejonie badań towarzyszyło typom cyrkulacji Sc+SWc+Wc i Sa+SWa+Wa (anomalie dodatnie od 7 do 9%), a najsuchsze (anomalie ujemne wahające się od 6% do 9%) podczas napływu mas powietrza z sektora wschodniego, niezależnie od rodzaju układu barycznego. Najmniejsze różnice (do ok. 1-2%) wystąpiły w sytuacjach bezadwekcyjnych reprezentowanych przez typ Ka+Ca.
This paper presents the spatial diversity of air relative humidity (2 m a.g.l.) in the northern part of the Kaffiøyra Plain and on the Waldemar Glacier (NW Spitsbergen), from September 2010 to August 2013, based on measurements taken at six sites located in different environments (Table 1, Figure 1). Results are described for years and seasons, defined as: autumn (Sep-Oct), winter (Nov-Mar), spring (Apr-May) and summer (Jun-Aug). In the period from September 2010 to August 2011, the highest relative humidity was noted on mountain ridges (89%) and in upper part of the Waldemar Glacier (86%). The lowest value of humidity (79%) occurred at a tundra site called ‘Terrace’, located about two kilometres from the coast (Table 2, Figure 2). In the entire period of observations, for which a reduced number (3) of observation sites exists, drier air (83%) was observed at the Kaffiøyra-Heggodden (KH) site, located in the terminal-lateral moraine of the Aavatsmark Glacier, whereas the wettest air (85%) was measured at the firn part of the Waldemar Glacier (LW2). Relative humidity generally shows an increase as altitude increases above sea level. The marked influence of atmospheric circulation on relative humidity was also noted. In the study period, as compared to long-term values from 1951 to 2006, a decrease in the frequency of occurrence of anticyclonic types and an increase in the frequency of cyclonic types (by 10% and 6.8%, respectively) was also noted (Figure 3). Most humid air in the study area occurred within the circulation types Sc+SWc+Wc and Sa+SWa+Wa (positive anomalies varied from 7% to 9%), and the driest (negative anomalies from 6% to 9%) during air advection from the eastern sector within both anticyclonic and cyclonic weather patterns (Table 3 and Figure 4). The smallest differences (up to 2%) were connected with non-advectional weather type Ka+Ca.
Źródło:
Problemy Klimatologii Polarnej; 2014, 24; 25-36
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie przestrzenne i wieloletnia zmienność temperatury gruntu w rejonie Stacji Polarnej UMK (NW Spitsbergen) w okresie letnim (1975-2009)
Differentiation and long-term changes in ground temperature on the Kaffioyra plan (NW Spitsbergen) in the summer season from 1975 to 2009
Autorzy:
Przybylak, R.
Araźny, A.
Kejna, M.
Powiązania:
https://bibliotekanauki.pl/articles/261005.pdf
Data publikacji:
2010
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Spitsbergen
temperatura gruntu
sezon letni
zmienność wieloletnia
ground temperature
summer season
long-term changes
Opis:
W artykule przedstawiono podsumowanie wyników badań dotyczących zmian temperatury gruntu w otoczeniu Stacji Polarnej UMK na Kaffioyrze (NW Spitsbergen) w sezonie letnim. Do analizy wzięto dane pomiarowe z 5 głębokości (1, 5, 10, 20 i 50 cm) z 3 różnych ekotopów (plaża, morena i tundra) wykonane w trakcie 17 dotychczasowych wypraw polarnych zorganizowanych przez Instytut Geografii UMK w różnych latach okresu 1975-2009. W celu uzyskania pełnej porównywalności wyników wybrano okres 21.07-31.08, dla którego dostępne są kompletne dane dla niemal wszystkich sezonów letnich analizowanych w artykule. Serie temperatury gruntu na wszystkich stanowiskach i poziomach są ze sobą bardzo silnie skorelowane. Wyraźnie największy wpływ na zmierzone wartości temperatury gruntu w całej badanej warstwie wywiera tempe-ratura powietrza (współczynniki korelacji wahają się od 0,6 do 0,86). Inne elementy meteorologiczne takie jak prędkość wiatru, zachmurzenie i usłonecznienie również w sposób istotny wpływają na temperaturę gruntu, ale głównie w warstwie 0-20 cm (współczynniki korelacji wahają się od 0,15 do 0,28). Istotny statystycznie, chociaż ilościowo bardzo niewielki, wpływ na temperaturę gruntu w warstwie do 20 cm ma także opad atmosferyczny.
In the present paper a comprehensive synthesis of ground temperature changes on the Kaffiřyra Plain (NW Spitsbergen) in the summer season (21st July to 31st August) from 1975 to 2009 is described. This has been done with two main aims in mind: i) to examine the influence of different ecotypes on ground temperature values in the layer 1-50 cm, and ii) to examine long-term changes of ground temperature. The highest values of long-term average ground temperature in the summer season have been observed between 20th and 25th July. After this period a gradual decrease in ground temperature is observed (Table 2, Fig. 3). One clear cold singularity can be distinguished here occurring at the end of July and start of August which is connected with a significant decrease in air temperature observed very often during this time. In the period 1978-2009 the warmest ground in the entire analysed layer was observed at the ‘Moraine’ site (6.2°C), and the coldest was at the ‘Tundra’ site (5.1°C) – Table 3, Fig. 4. However, in the shallowest layer (up to 1 cm) markedly the warmest site was the beach, while the coldest was at a depth of 50 cm (Fig. 4). The reason for the large decrease of temperature in this layer was that this was where the permafrost roof was at its shallowest. As a consequence of this temperature behaviour in the layer, the ‘Beach’ site shows the greatest lapse rate of ground temperature (-0.78°C/10 cm) (Table 4). In the warmest summer seasons a greater range of ground temperature in the daily cycle is observed than in the coldest ones, which is very clearly seen, in particular in the layer from surface up to 20 cm (Fig. 5). In the study period a significant increase in ground temperature in the layer 1-20 cm was observed starting in 1998, while at a depth of 50 cm this rise can be seen from 2005 onward (Fig. 6). Very high and statistically significant correlation have been found between series of daily ground temperature taken from all sites and all measurement depths (Table 5). Air temperature is a meteorological variable, which has the greatest influence on the values of ground temperature. Correlation coefficients between series of its daily values and series of average daily ground temperature in all analysed depths at the ‘Beach’ site oscillate from 0.6 to 0.86 (Table 6, Fig. 7). Important factors controlling values of ground temperature in the layer 0-20 cm are also wind velocity, cloudiness and sunshine duration (correlation coefficients oscillate between 0.15 and 0.28).
Źródło:
Problemy Klimatologii Polarnej; 2010, 20; 103-120
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie opadów atmosferycznych w rejonie Kaffioyry (NW Spitsbergen) w sezonie letnim w latach 1980-2008
Atmospheric precipitation differentiation in the Kaffioyra region (NW Spitsbergen) in summer season, 1980-2008
Autorzy:
Przybylak, R.
Araźny, A.
Kejna, M.
Maszewski, R.
Wyszyński, P.
Powiązania:
https://bibliotekanauki.pl/articles/260663.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Spitsbergen
Kaffioyra
sezon letni
opady atmosferyczne
cyrkulacja atmosferyczna
summer season
precipitation
atmospheric circulation
Opis:
W opracowaniu przedstawiono zróżnicowanie warunków opadowych w rejonie Kaffioyry (NW Spitsbergen) w sezonie letnim na podstawie danych z lat 1980-2008. Zbadano wpływ cyrkulacji atmosferycznej i warunków lokalnych na opady atmosferyczne. Uzyskane wyniki porównano ze stacją Ny-Alesund.
Precipitation in the Arctic, including Spitsbergen, is very important for both the biosphere and for the mass balance of glaciers. Our knowledge about its values inside Arctic islands is limited because almost all meteorological stations are located on tundra below 200 m a.s.l. Therefore any information about precipitation conditions occurring on glaciated and non-glaciated areas lying in the inner parts of Spitsbergen is very valuable. In this paper we present results of precipitation measurements carried out in north-western Spitsbergen (the Kaffioyra region and the Ny Alesund station) in selected summer seasons during the period 1980-2008. Precipitation measurements in the Kaffioyra region have been done during Toruń Polar Expeditions in three stations (base station – Kaffioyra-Heggodden (KH) and two glacier stations located in the lower part (LW1) and upper part (LW2) (see Figure 1 and Table 1). Data for the Ny Alesund (NA) station were obtained from the Norwegian Meteorological Institute. In the KH and NA stations measurements were recorded every day, while in LW1 and LW2 they were generally taken every 1-2 days. Results of precipitation conditions are presented for a common period of observations, i. e. for 21st July-31st August. The influence of atmospheric circulation on precipitation was investigated using the catalogue of circulation types constructed by Niedźwiedź (2009). In the summer season precipitation is greater at the end of the study period, than at the beginning. Year-to-year variability of summer precipitation totals is very large. For example, in KH, the highest precipitation (122.5 mm) occurred in 1997, while the lowest (12.3 mm) was in 2007 (Table 2). Also, the frequency of daily precipitation (.0.1 mm) is significantly greater in most wet summer (61.9%) than in most dry summer (28.6%) (see Table 3). Daily precipitation of .10 mm is rare in the KH station and occurred in only 4 out of the 12 summer seasons. It is well known that precipitation is greater in the inner parts of Spitsbergen than in tundra areas. Less is known, however, about the magnitudes of these differences. For the Kaffioyra region precipi-tation observations are available for 9 summer seasons (Tables 5 and 6). From these Tables and Figure 2 it is clear that precipitation on glaciers is almost always greater than in tundra. On average, summer precipitation totals are greater in LW1 and LW2 than in KH by 21.5 and 35.1 mm, respectively. The greatest differences occurred in 1980, while the lowest were in 2007, when even in LW1 precipitation was lower than in KH (Table 5, Figure 3). Lapse rates of precipitation in the Kaffioyra region are greatest between tundra and glaciated areas (oscillating between 13.2mm/100m and 18.5mm/100m between KH and LW2 and KH and LW1, respectively (Table 7)). On the other hand, this lapse rate between stations LW1 and LW2 is the lowest (only 10.7 mm/100 m). Correlation coefficients of 10-day precipitation totals between the meteorological stations in the Kaffioyra region are very high and exceed 0.9. The greatest precipitation in the Kaffioyra region occurred during the inflow of air masses from the southern sector (Table 8, Fig. 7).
Źródło:
Problemy Klimatologii Polarnej; 2009, 19; 189-202
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie albedo Lodowca Scotta (W Spitsbergen)
The 'Albedo' differentiation at Scott's Glacier (W Spitsbergen)
Autorzy:
Siwek, K.
Gluza, A.
Bartoszewski, S.
Powiązania:
https://bibliotekanauki.pl/articles/260684.pdf
Data publikacji:
2004
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
pokrywa śnieżna
ablacja
Lodowiec Scotta
Spitsbergen
snow cover
ablation
Scott's Glacier
Opis:
The aim of the present study was the quantitative determination of ?albedo? which is a significant factor influencing the balance of short-wave radiation. The value of surface albedo allows to determine its role in the heat balance of the active surface which in turns influences the ablation level. Studies on the accumulation and ablation conditions of the snow cover commenced on Scott?s Glacier in 1987. On average, the thickness of the frontal part decreased by 75 m, i.e. 2.7 m annually. Decession of the glacier was confirmed by studies carried out in 2001 during which it was found that Scott?s Glacier had decreased in its surface area by over 10% in the period 1986?2001. Three types of active surfaces, i.e.: land, ice and water, play a significant role in the radiation balance of the Arctic. During the summer months practically all the heat reaching the surface of the earth is taken up in thawing the ice. In the summer of 2001, a substantial variation of albedo occurred on Scott?s Glacier. The above changes depended to a large extent on the physical properties of the glacier?s surface. High spatial differentiation of albedo was also observed in the period studied (i.e. the summer of 2001). The lowest values (15-25%) occurred at the front of the glacier which was covered with ice and numerous kryokonite smelts filled with water or polluted with morenic or eolic material. Somewhat higher values (40-60%) were found in the supraglacial river valleys and in the zone of surface water deposits as they turned into slush. The highest albedo values occurred in the firn field where leveled snow, often firn, or fresh wind-blown snow was deposited (60-85%). After the precipitation of the fresh, clean snow, albedo increased and reached values above 88%.
Źródło:
Problemy Klimatologii Polarnej; 2004, 14; 127-132
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie albedo Calypsostrandy (Zachodni Spitsbergen) w sezonie letnim 2001
The albedo differentation at Calypsostranda (W Spitsbergen) in summer season 2001
Autorzy:
Gluza, A.
Siwek, K.
Powiązania:
https://bibliotekanauki.pl/articles/260860.pdf
Data publikacji:
2005
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
albedo
tundra
pomiary patrolowe
Calypsostranda
Spitsbergen
patrol measurement
Opis:
W pracy przedstawiono zróżnicowanie albedo wybranych ekosystemów Calypsostrandy - płaskiej równiny nadmorskiej położonej w NW części Ziemi Wedela Jarlsberga (Spitsbergen). Pomiary prowadzono w sezonie letnim 2001, metodą patrolową w godzinach okołopołudniowych ze względu na najmniejsze zmiany kąta padania promieni słonecznych. Analizie poddano zróżnicowanie albedo w dwóch dniach znacznie różniących się stopniem zachmurzenia nieba.
The aim of the present study was the quantitative determination of 'albedo' which is a significant factor influencing on the balance of short-wave radiation. The value of surface albedo allows determining its role in the heat balance of the active surface. The area of investigations is situated in the NW part of Wedel Jarlsberg Land in the Bellsund region on the Western Spitsbergen. Calypsostranda is the fragment of the regional unit, representing the type of marine coastal plain. Calypsostranda is situated on the forefield of the Scott and Renard Glaciers. It is complex of raised marine terraces with highs 3-100 m. The greatest area is occupied by terraces 20-40 m. a.s.l. Calypsostranda is formed by series of boulder clays, fluvioglacial sands, and gravels as well as by marine sands, gravels and silts. The dominant plant formation on Calypsostranda is dry lichen-moss tundra. The local differentiation of plant cover which exists there is implied by the kind of background and water relations. Lichen tundra is dominated by very dry habitats. When the humidity of ground increases the phyla appear in the water. There were three types of active surfaces, i.e.: land, ice and water, play a significant role in the radiation balance of the Calypsostranda. In the summer of 2001, a substantial variation of albedo occurred on Calypsostranda. The above changes depended to a large extent on the physical properties of the tundra?s surface. High spatial differentiation of albedo was also observed in the studied period (i.e. the summer of 2001). The Iowest values (below 10%) occurred at the lakelet area with dark bottom polluted with eolic material. The highest albedo values (above 20%) were noticed in the patterned grounds and on the beach. The average albedo for the tundra area (for all measurement period) is 15.5% and it was changed from 11% to 21%.
Źródło:
Problemy Klimatologii Polarnej; 2005, 15; 113-117
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zooplankton structure in high latitude fjords with contrasting oceanography (Hornsund and Kongsfjorden, Spitsbergen)
Autorzy:
Ormanczyk, M.R.
Gluchowska, M.
Olszewska, A.
Kwasniewski, S.
Powiązania:
https://bibliotekanauki.pl/articles/47860.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
zooplankton
stock size
Hornsund Region
Kongsfjorden
Spitsbergen
taxonomic composition
size structure
biogeography
hydrography
trophic relation
Atlantic water
environment change
Opis:
Zooplankton inhabiting the Hornsund and Kongsfjorden fjords on Spitsbergen (Svalbard) were investigated in summer 2013. The goal of the study was to determine how the zooplankton communities vary in environments functioning under different oceanographic regimes. Sampling was conducted with nets of different mesh size and selectivity (56 μm WP-2, 180 μm MultiNet, and 1000 μm Tucker Trawl), which permitted comparing a wide size spectrum of zooplankton components. Species composition did not differ substantially between the fjords, but the zooplankton in Hornsund was almost two times less numerous, and it had lower biomass per unit volume. The highest abundance at both sites was in the smallest zooplankton size fraction found only in samples taken with 56 μm mesh WP-2 net. These comprised as much as 71% and 58% of the total zooplankton abundance in Hornsund and Kongsfjorden, respectively. The communities in both fjords had comparable contributions of Arctic and boreo-Arctic species biomass in the year of the study. However, the comparison of zooplankton characteristics over several years showed changes in abundance and biogeographic structure that corresponded with variations in the physical environments of the fjords. The results of the study permit predicting the possible effects of the increasing influence of Atlantic waters on zooplankton communities inhabiting Arctic marine pelagic ecosystems.
Źródło:
Oceanologia; 2017, 59, 4
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Znaczenie badań naukowych dla gospodarki Svalbardu
Autorzy:
Legutko, Agnieszka Joanna
Powiązania:
https://bibliotekanauki.pl/articles/624583.pdf
Data publikacji:
2017
Wydawca:
Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
Tematy:
Svalbard, Spitsbergen, economy of Svalbard, polar research in Svalbard, University Centre in Svalbard, coal industry in Svalbard
Svalbard, Spitsbergen, gospodarka Svalbardu, badania polarne na Svalbardzie, przemysł wydobywczy na Svalbardzie, Centrum Uniwersyteckie Svalbard
Opis:
The aim of the following paper is to present ongoing changes in Svalbard’s economy and to emphasize influence of scientific research for specific economic structure of the archipelago. To start with, author briefly describes main periods in history of this area, though the main focus is on present situation, so downturn of coal mining along with growing presence of scientists, development of University Centre in Svalbard and popularization of polar tourism. Thanks to combining quantitative methods, as well as direct observation and interviews with inhabitants during author’s stay in Svalbard in summer 2015, the paper answers the research question how does polar research influences Svalbard’s economy.
Celem poniższego artykułu jest przedstawienie aktualnych zmian w sytuacji ekonomicznej Svalbardu oraz podkreślenie wpływu badań naukowych na szczególną strukturę gospodarczą archipelagu. Na początku autorka krótko opisuje główne okresy w historii tego obszaru, jednak główny nacisk jest położony na bieżącą sytuację, a więc spadki w przemyśle wydobywczym przy jednoczesnym wzroście obecności naukowców, rozwoju Centrum Uniwersyteckiego na Svalbardzie, a także rosnącej roli turystyki polarnej. Dzięki zastosowaniu metod ilościowych, a także bezpośredniej obserwacji i wywiadów z mieszkańcami podczas pobytu autorki na archipelagu latem 2015 r., opracowanie odpowiada na pytanie badawcze, w jaki sposób badania polarne wpływają na gospodarkę Svalbardu.
Źródło:
Teka Komisji Politologii i Stosunków Międzynarodowych; 2017, 12, 2
1896-8279
Pojawia się w:
Teka Komisji Politologii i Stosunków Międzynarodowych
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność występowania opadów deszczu i śniegu w Hornsundzie w okresie lipiec 1978 - grudzień 2002
Variability in the occurrence of rain and snow at Hornsund over the period July 1978 - December 2002
Autorzy:
Łupikasza, E.
Powiązania:
https://bibliotekanauki.pl/articles/260943.pdf
Data publikacji:
2003
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Spitsbergen
opady atmosferyczne
opady deszczu
opady śniegu
rain
snow
Opis:
In the polar regions, the sums of precipitation of the accumulation period is of great importance, because they are an component one of the most valid processes connected with glacier mass balance - accumulation. From glaciological point of view, to determine which part of annual sums of precipitation appears in the form liquid and mixed and solid precipitation is the crucial problem. In this connection, the main aim of this paper is analyse variability of the precipitation with respect of their form in the annual course as well as their long-term variability in Hornsund in the period of 1978-2002. The data used in this article are mainly derived from meteorological yearbook Hornsund (2000, 2001) that was published by Institute of Meteorology and Water Management - maritime department in Gdynia and from yearbook Meteorological Conditions Hornsund, Spitsbergen (2001) that was published by Polish Academy of Science in Warsaw. Collected numerical data are not complete. There is a lack of data concerned precipitation sums and meteorological phenomenon for the period from 01sth to 26sth of July 1981. Moreover the data describing precipitation sums does not exist for the days: 04, 07, 09, 19 July 1979. In this article three main form of precipitation (liquid, mixed and solid) were considered. The form of precipitation was determined on the base of meteorological phenomenon that was recorded as current and last weather. The average, maximum and minimum daily air temperatures were additional criterions. In this connection that the notation of meteorological data prevented to consider each event of appearance of precipitation, the days with individual form of precipitation were subjected to analysis. The day with mixed precipitation means that during all 24 hour period (from 6 given to 6 next day) appeared one time snow and second time rain or snow and rain in the same time. The annual course of individual form of precipitation and their probability of appearance in each month, long term variability of sums of individual form of precipitation and the number of days with this form of precipitation in the accumulation and annual periods were discussed. The linear trends and variability coefficients were calculated for long term characteristics of precipitation. It was stated that in Hornsund long-term average sum of annual precipitation amounted at about 424 mm The greatest part of this appear in the liquid (37%) and the lowest in a mixed form. On average in Hornsund there is noted at about 239 days with precipitation in year from what 63% falls on days with snow and 13% on days with snow and rain. In the accumulation period the solid precipitation were characterized by greatest sums as well as greatest number of days with this one. Long-term course of individual form of precipitation shows similar tendencies. In the annual period as well as in the accumulation this one liquid precipitation are characterized by the highest variability coefficient and range of change. Their lowest sums occur in the middle of 80ies and from mid-80ies they show increasing tendency. Mixed precipitation shows the smallest range of change, their highest sums occur in the middle of 80ies and in the case of annual period also in the second half of 90ies. From the second half of 90ies mixed precipitation show decreasing tendency. Statistically significant increasing tendencies of liquid and mixed precipitation during all considered period accompany decreasing tendency of solid precipitation. The highest sums of solid precipitation occur in the first half of 80ies and the lowest one in the second half of the same decade. From the beginning of 90ies there is a decreasing tendency in the course of solid precipitation. During all considered period the solid precipitation dominate as regards number of days with precipitation. The number of days with solid precipitation until the end of 80ies was greater and in the 90ies was lower than long-term average.
Źródło:
Problemy Klimatologii Polarnej; 2003, 13; 93-105
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność warunków meteorologicznych w Hornsundzie (SW Spitsbergen) w okresie 1 VII 1999 - 30 VI 2000 roku
Variability of meteorological conditions at Hornsund (SW Spitsbergen) in the period from 1st July 1999 to 30th June 2000
Autorzy:
Araźny, A.
Powiązania:
https://bibliotekanauki.pl/articles/260790.pdf
Data publikacji:
2000
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
badania meteorologiczne
Spitsbergen
Hornsund
Opis:
Measurements and meteorological observations at Hornsund were carried out in the frame of the 22nd Polish Polar Expedition "Spitsbergen 1999/2000" research work. This was the consecutive year-long expedition organized by the Geophysical Institute of the Polish Academy of Sciences. Circulation factors have a great influence on the meteorological conditions at Hornsund. The mean annual atmospheric pressure at the sea level (1005.0 hPa) was lower than its long-term average. The mean wind velocity was 5.8 m/s. There were 971.9 hours with sunshine. The analysed year was characterised by high air temperature as for the Arctic conditions. The mean annual air temperature was -3.7°C, and was 1.1OChigher then its long-term average. The analysis of the air temperature trend in the period 1978-2000 shows a systematic warming about 0.07°C/year on the southern Spitsbergen. The annual sum of precipitation was 500.9 mm, i.e. about 77 mm higher then the long-term average. In September the highest monthly precipitation sum (230.0 mm) was measured till now.
Źródło:
Problemy Klimatologii Polarnej; 2000, 10; 55-72
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność temperatury powierzchni morza w rejonie Spitsbergenu (1982-2002) jako przejaw współcześnie zachodzących zmian klimatycznych
Changeability in sea surface temperature in the region of Spitsbergen (1982-2002) reflecting climatic changes observed at present
Autorzy:
Kruszewski, G.
Powiązania:
https://bibliotekanauki.pl/articles/260692.pdf
Data publikacji:
2004
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
temperatury powierzchni morza
zmiany klimatyczne
Spitsbergen
temperatury powietrza
sea surface temperature
climatic changes
air temperature
Opis:
This work has analysed changeability in water surface temperature in sea areas in the direct vicinity of West Spitsbergen. (Fig. 1). The analysis made use of SST (Sea Surface Temperature) from Reynolds?s data, covering mean monthly values of grids 1 x 1° from the period 1982-2002 (21 years). The changes in SST have been examined both monthly and yearly in 48 grids originating from the region 76-80°N, 006-020°E. A noticeable increase in water temperature was noted in the entire analysed area. The highest positive annual trends in water temperature were noted in the region 77-78°N, 006-007°E located west of Spitsbergen. In this area the mean yearly trends in SST values exceed +0.11°C/year and are highly statistically relevant (p<0.001). The values of trend noted in the areas in the direct vicinity of SW coast of Spitsbergen are +0.07°C to +0.08°C/year (at the latitudes 76-78°N). Farther north the values of the trend are remarkably lower, yet they are still highly statistically relevant. At 80°N the SST trend ranges from +0.006°C to +0.013°C and grows when moving west. At 79°N the observed trend of mean yearly value of SST is within the range from +0.04°C (010°E) to +0.07°C/year (006°E). This indicates that the mean yearly temperature of water in the region west of Spitsbergen has increased by more than 2.5°C over the period of the last 21 years and in coastal waters SW of Spitsbergen by about 1.5°C to 1.7°C. The lowest increase in SST was noted in waters at 80°N, where it did not exceed 0.3°C within 21 years. The increase in water temperature is distributed unevenly in time - since 1995 the rate of the increase has been rapidly growing (see Fig. 2). The changes in yearly SST values, as the analysis indicated, are influenced by the changes in temperature noted mainly in the period from September to February. This proves that the heat sources carried by the West Spitsbergen Current are increasing and that the summer warming of waters is becoming more and more significant. Interannual changeability in SST in the remaining months proves to be relatively low, in extreme cases being zero (water completely frozen). It can be observed especially at 80°N. The yearly changeability in values of SST in waters around SE coasts of Spitsbergen (Storfjorden) is mainly influenced by the temperature of waters in autumn (August ? October), which means that the influence of the summer warming of waters on the yearly SST value in this area has increased.
Źródło:
Problemy Klimatologii Polarnej; 2004, 14; 79-86
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność opadów atmosferycznych w Hornsundzie (Spitsbergen) w okresie 1978-2000
The variation of the atmospheric precipitation in Hornsund (Spitsbergen) in the period 1978-2000
Autorzy:
Łupikasza, E.
Powiązania:
https://bibliotekanauki.pl/articles/260909.pdf
Data publikacji:
2002
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Spitsbergen
opady atmosferyczne
precipitation
Opis:
In the polar area, the precipitation is a component of one of the most important processes connected with the glacier mass balance ? accumulation and ablation. In this case particular signifi-cance is attributed to the height of the precipitation for a month of a cool season. The aim of this study is to examine the long-term variability of the atmospheric precipitation in Hornsund by the analysis of the monthly, seasonal and annual sums of precipitation and the sums of the precipitation for the accumulation season. Moreover, the long-term variability of the frequency of the days with precipitation (>= 0.0 mm), of the days with trace precipitation (= 0.0 mm), of the days with the precipitation >= 0.1 mm, >= 1.0 mm, >= 5.0 mm, >= 10.0 mm, >= 20.0 mm was discussed in the scale of the year, seasons and the accumulation period. The investigation of long-term variability of the precipitation in Hornsund that was carried out indicated that annual sums of precipitation amount to 421.7 mm. The annual sums of the precipitation are distinguished by the rising tendency showing up from the beginning of the measurement period to 1995. In the second half of the 90-ties, despite of high sums, annual precipitation is characterised by decreasing tendency that is connected with the low sums of precipitation in 1998. The highest part of annual precipitation falls in autumn and slightly less in summer. The lowest precipitation sums appear in spring. A slightly decreasing tendency is visible in the long-term course of spring precipitation. Both the autumn and the summer precipitation is characterised by the higher sums in the last decade of the 20th century than in the earlier period. Moreover, the autumn sums of precipitation are distin-guished by an increasing trend in the last decade of the 20th century while the course of summer precipitation shows the decreasing tendency from 1994. Taking into consideration the monthly values it was stated that September predominates in respect of the height of precipitation. High precipitation also occurs in August. The lowest sums of the monthly precipitation occur in the end of winter and in spring, with especially low sums in May and April. The long-term course of precipitation in particular months is diverse and exhibits specific features. The frequency of the days with defined thresholds of precipitation sums exhibits a great diversity of long-term course in the considered scales of time. The period in the turn of the 80-ties and 90-ties is interesting from the point of view of temporary variability of the frequency of precipitation. In this period the highest frequencies of the days with defined thresholds of precipitation sums often occured or the change of tendencies direction took place.
Źródło:
Problemy Klimatologii Polarnej; 2002, 12; 77-88
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 391

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